The role of Internal Solitary Waves on deep-water sedimentary processes: the case of up-slope migrating sediment waves off the Messina Strait

Subaqueous, asymmetric sand waves are typically observed in marine channel/canyon systems, tidal environments, and continental slopes exposed to strong currents, where they are formed by current shear resulting from a dominant unidirectional flow. However, sand-wave fields may be readily observed in...

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Detalles Bibliográficos
Autores principales: Droghei, R., Falcini, F., Casalbore, D., Martorelli, E., Mosetti, R., Sannino, G., Santoleri, R., Chiocci, F. L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5093411/
https://www.ncbi.nlm.nih.gov/pubmed/27808239
http://dx.doi.org/10.1038/srep36376

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5093411/
https://www.ncbi.nlm.nih.gov/pubmed/27808239
http://dx.doi.org/10.1038/srep36376

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